Multi-stage hydrothermal processes involved in “low-sulfide” Cu(–Ni)–PGE mineralization in the footwall of the Sudbury Igneous Complex (Canada): Amy Lake PGE zone, East Range-Reference-Cited by-同舟云学术

Multi-stage hydrothermal processes involved in “low-sulfide” Cu(–Ni)–PGE mineralization in the footwall of the Sudbury Igneous Complex (Canada): Amy Lake PGE zone, East Range

Published:2013-05-09 Issue:1 Volume:49 Page:7-47
ISSN:0026-4598
Container-title:Mineralium Deposita
language:en
Short-container-title:Miner Deposita

Author:

Tuba Györgyi,Molnár Ferenc,Ames Doreen E.,Péntek Attila,Watkinson David H.,Jones Peter C.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics,Economic Geology

Link

http://link.springer.com/content/pdf/10.1007/s00126-013-0468-1.pdf

Reference106 articles.

1. Ames DE, Farrow CEG (2007) Metallogeny of the Sudbury mining camp, Ontario. In Goodfellow WD (ed) Mineral deposits of Canada: A synthesis of major deposit-types, district metallogeny, the evolution of geological provinces, and exploration methods. GAC Mineral Deposits Division Special Publication 5:329–350

2. Ames DE, Watkinson DH, Parrish RR (1998) Dating of a regional hydrothermal system induced by the 1850 Ma Sudbury impact event. Geology 26:447–450

3. Ames DE, Golightly JP, Lightfoot PC, Gibson HL (2002) Vitric compositions in the Onaping Formation and their relationship to the Sudbury Igneous Complex, Sudbury structure. Econ Geol 97:1541–1562

4. Ames DE, McClenaghan MB, Averill S (2007) Footwall-hosted Cu-PGE (Au, Ag), Sudbury Canada: Towards a new exploration vector (abs). Fifth Decentennial International Conference on Mineral Exploration, September 2007, Toronto, Canada

5. Ames DE, Davidson A, Wodicka N (2008) Geology of the giant Sudbury polymetallic mining camp, Ontario, Canada. Econ Geol 103:1057–1077

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